-
BASIS 1998 - Baltic Air Sea Ice Study 1998: meteorological measurements of th...
The field experiment BASIS 1998 took place in the Gulf of Bothnia in the Baltic Sea in a boundary zone between the open sea and the ice-covered sea from 16 February to 7 March,... -
ARKTIS 1993 - Air mass modification and convection in off-ice air flows over ...
The field experiment ARKTIS 1993 was the third one in a series of experiments in the Arctic region performed by a group of climate researchers from Hamburg. The campaign took... -
ARKTIS 1991 - Cellular Convection over the Norwegian Sea: radiosoundings at t...
The field experiment ARKTIS 1991 was an expedition planned by meteorologists of the Collaborative Research Centre 318 entitled "Climatically relevant processes in the system... -
ARKTIS 1988 - Atmospheric Boundary Layer in the Marginal Ice Zone in the Fram...
The expedition ARKTIS 1988 was initiated and directed by the Collaborative Research Centre 318 of the German Research Foundation entitled "Climatically relevant proceses in the... -
ALKOR 2001 - Three RV Alkor cruises to the central Baltic Sea 2001: radiosoun...
The field experiments ALKOR 2000 (consisting of three cruises: ALKOR 4/2000, 6/2000, 10/2000) and ALKOR 2001 (4/2001, 6/2001, 10/2001) took place in the central Baltic Sea. The... -
ALKOR 2000 - Three RV Alkor cruises to the central Baltic Sea 2000: radiosoun...
The field experiments ALKOR 2000 (consisting of three cruises: ALKOR 4/2000, 6/2000, 10/2000) and ALKOR 2001 (4/2001, 6/2001, 10/2001) took place in the central Baltic Sea. The... -
ACSYS 2003 - Arctic Atmospheric Boundary Layer and Sea Ice Interaction Study ...
From 26 March to 22 April 2003, Germany and Finland carried out a joint expedition (ABSIS - Arctic Atmospheric Boundary Layer and Sea Ice Interaction Study) to test and improve... -
Climate Simulation with CLM, Scenario A1B run no.1, North Atlantic region
The experiment CLM_A1B_ZS contains Northern European regional climate simulations of the years 2070-2099 on a rotated grid (CLM non hydrostatic, 0.44 deg. hor. resolution, see... -
Climate Simulation with CLM, Scenario 20C run no.1, North Atlantic region
The experiment CLM_20C_ZS contains Northern European regional climate simulations of the years 1960-1989 on a rotated grid (CLM non hydrostatic, 0.44 deg. hor. resolution, see... -
Climate Simulation with CLM, Scenario B1 run no.1, North Atlantic region
The experiment CLM_B1_ZS contains Northern European regional climate simulations of the years 2070-2099 on a rotated grid (CLM non hydrostatic, 0.44 deg. hor. resolution, see... -
Climate Simulation with CLM, Scenario A2 run no.1, North Atlantic region
The experiment CLM_A2_ZS contains Northern European regional climate simulations of the years 2070-2099 on a rotated grid (CLM non hydrostatic, 0.44 deg. hor. resolution, see... -
dphase_larsimby: hydrological model LARSIM (Bavaria) forecasts run by WWA-KE ...
Hydrological forecasts with hydrological model LARSIM (LARSIM=LArge Area Runoof Simulation Model, BY=Bavaria, Conceptual RR-model. Forecast depth: 72 hours.) for rivers Iller... -
dphase_larsimbw: hydrological model LARSIM (Baden-Wuerttemberg) forecasts run...
LARSIM (LARSIM=LArge Area Runoff Simulation Model BW= Baden-Wuerttemberg) is described in "Freiburger Schriften zur Hydrologie", Band 22. 2006 (Ludwig, K.; Bremicker, M.: The... -
dphase_fest: hydrological model FEST run by Politecnico di Milano for the MAP...
The goal of the experiment is to drive FEST, a rainfall-runoff distributed model with continuous soil moisture account, with ensemble forecasts from COSMO-LEPS (CLEPS) and with... -
dphase_dimosop: hydrological model DIMOSOP run by University of Brescia for t...
The hydrological model DIMOSOP was run by University of Brescia with three different atmospheric forcings and different runoff forecast times. For more... -
dphase_hbv: hydrological model HBV runoff forecasts in the Rhine basin run by...
FOEN is using the Flood Early Warning System (FEWS) with the hydrological model HBV for operational flood forecasts in the swiss part of the Rhine basin. With respect to MAP... -
Reconstruction of global land use and land cover AD 800 to 1992
This dataset contains reconstructions of land use and land cover from AD 800 to 1992 in global coverage at 30 minute resolution. After AD 1700, the data is based on Ramankutty... -
dphase_mesonh8: Meso-NH forecasts (8km) run by University of Toulouse for the...
The horizontal grid spacing is here 8 km. The domain size is 160 x 108 gridpoints covering the MAP D-PHASE domain. The vertical grid has 50 levels up to 20... -
dphase_mesonh2: Meso-NH forecasts (2km) run by University of Toulouse for the...
The horizontal grid spacing for MESONH is here 2 km. The domain size is 192 x 180 gridpoints covering the COPS area. The vertical grid has 50 levels up to... -
dphase_lmeuro: COSMO-ME model forecasts (7km) run by Italian Met. Service CNM...
COSMO-ME is the high-resolution operational implementation of COSMO Model at the National Meteorological Service of Italy. The model domain covers most of...